Atmospheric Moisture
1. The highest relative humidity for the day
is usually around sunrise when the air temperature is coolest. is usually later in the afternoon when the air temperature is the warmest. is right at noon is at midnight
2. If the temperature of the air increases without additional water vapor being added to the air the relative humidity will likely
increase decrease stay the same temperature has no impact on relative humidity
3. On a day in mid-June a parcel of air and the air that surrounds it at ground level are found to have the same temperature. You also find that the ELR is greater than the DAR on that day. If the parcel is given an upward push
the air would be stable the air would be unstable the parcel and surrounding air will still have the same temperature none of the above
4. A fog that forms when warm, moist air comes in contact with a cool surface is called
a steam fog an upslope fog a radiation fog an advection fog
5. The ice crystal growth model
applies to cold clouds applies to mid and high latitude situations requires the presence of super-cooled water all the above
6. The weight of water vapor per unit weight of dry air is
the mixing ratio the relative humidity the absolute humidity the vapor pressure
7. Thin, wispy high clouds composed of ice crystals are
cumulus clouds cirrus clouds stratus clouds cumulonimbus clouds
8. Latent heat
is stored in water molecules when condensation occurs is converted to sensible heat when water vapor condenses is used to raise the temperature of the water relates to none of the above
9. Radiation fog
is more likely to form during the day is more likely to form at night forms when it is windy none of the above
10. Frost is a product of
evaporation condensation sublimation deposition
Score = Correct answers:
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For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography. Date visited. https://www.thephysicalenvironment.com/
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